A Laboratory For Star Formation

The Great Conjunction of Jupiter and Saturn

Credits:  NASA/Bill Ingalls

Have you noticed two bright objects in the sky getting closer together with each passing night? It’s Jupiter and Saturn doing a planetary dance that will result in the Great Conjunction on Dec. 21. On that day, Jupiter and Saturn will be right next to each other in the sky – the closest they have appeared in nearly 400 years!

Skywatching Tips from NASA

Credits: NASA/JPL-Caltech

For those who would like to see this phenomenon for themselves, here’s what to do:

Find a spot with an unobstructed view of the sky, such as a field or park. Jupiter and Saturn are bright, so they can be seen even from most cities.

An hour after sunset, look to the southwestern sky. Jupiter will look like a bright star and be easily visible. Saturn will be slightly fainter and will appear slightly above and to the left of Jupiter until December 21, when Jupiter will overtake it and they will reverse positions in the sky.

The planets can be seen with the unaided eye, but if you have binoculars or a small telescope, you may be able to see Jupiter’s four large moons orbiting the giant planet.

How to Photograph the Conjunction

Credits: NASA/Bill Dunford

Saturn and Jupiter are easy to see without special equipment, and can be photographed easily on DSLR cameras and many cell phone cameras. Here are a few tips and tricks:

These planets are visible in the early evening, and you'll have about 1-2 hours from when they are visible, to when they set. A photo from the same location can look completely different just an hour later!

Using a tripod will help you hold your camera steady while taking longer exposures. If you don’t have a tripod, brace your camera against something – a tree, a fence, or a car can all serve as a tripod for a several-second exposure.

The crescent Moon will pass near Jupiter and Saturn a few days before the conjunction. Take advantage of it in your composition!

Get more tips HERE.

Still have questions about the Great Conjunction?

Our NASA expert answered questions from social media on an episode of NASA Science Live on Thursday, Dec. 17. Watch the recording HERE.

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Five Eclipses in NASA History

On Monday, August 21, 2017, people in North America will have the chance to see an eclipse of the Sun. Anyone within the path of totality may see one of nature’s most awe-inspiring sights – a total solar eclipse. 

Along this path, the Moon will completely cover the Sun, revealing the Sun’s tenuous atmosphere, the corona. The path of totality will stretch from Salem, Oregon, to Charleston, South Carolina. Observers outside this path will still see a partial solar eclipse, where the Moon covers part of the Sun’s disk. Remember: you can never look at the Sun directly, and an eclipse is no exception – be sure to use a solar filter or indirect viewing method to watch partial phases of the eclipse.

Total solar eclipses are a rare chance to study the Sun and Earth in unique ways. During the total eclipse, scientists can observe the faintest regions of the Sun, as well as study the Sun’s effects on Earth’s upper atmosphere. We’ve been using eclipses to learn more about our solar system for more than 50 years. Let’s take a look back at five notable eclipses of the past five decades.

May 30, 1965

A total eclipse crossed the Pacific Ocean on May 30, 1965, starting near the northern tip of New Zealand and ending in Peru. Totality – when the Moon blocks all of the Sun’s face – lasted for 5 minutes and 15 seconds at peak, making this the 3rd-longest solar eclipse totality in the 20th century. Mexico and parts of the Southwestern United States saw a partial solar eclipse, meaning the Moon only blocked part of the Sun. We sent scientists to the path of totality, stationing researchers on South Pacific islands to study the response of the upper atmosphere and ionosphere to the eclipse. 

Additionally, our high-flying jets, scientific balloons, and sounding rockets – suborbital research rockets that fly and collect data for only a few minutes – recorded data in different parts of the atmosphere. A Convair 990 research jet chased the Moon’s shadow as it crossed Earth’s surface, extending totality up to more than nine minutes, and giving scientists aboard more time to collect data. A NASA-funded team of researchers will use the same tactic with two jets to extend totality to more than 7 minutes on Aug. 21, 2017, up from the 2 minutes and 40 seconds observable on the ground. 

March 7, 1970

The total solar eclipse of March 7, 1970, was visible in North America and the northwestern part of South America, with totality stretching to 3 minutes and 28 seconds at maximum. This was the first time a total eclipse in the United States passed over a permanent rocket launch facility – NASA’s Wallops Station (now Wallops Flight Facility) on the coast of Virginia. This eclipse offered scientists from NASA, four universities and seven other research organizations a unique way to conduct meteorology, ionospheric and solar physics experiments using 32 sounding rockets. 

Also during this eclipse, the Space Electric Propulsion Test, or SERT, mission temporarily shut down because of the lack of sunlight. The experimental spacecraft was unable to restart for two days.

July 10, 1972

Two years later, North America saw another total solar eclipse. This time, totality lasted 2 minutes and 36 seconds at the longest. A pair of scientists from Marshall Space Flight Center in Huntsville, Alabama, traveled to the Canadian tundra to study the eclipse – specifically, a phenomenon called shadow bands. These are among the most ephemeral phenomena that observers see during the few minutes before and after a total solar eclipse. They appear as a multitude of faint rapidly moving bands that can be seen against a white background, such as a large piece of paper on the ground. 

While the details of what causes the bands are not completely understood, the simplest explanation is that they arise from atmospheric turbulence. When light rays pass through eddies in the atmosphere, they are refracted, creating shadow bands.

February 26, 1979

The last total solar eclipse of the 20th century in the contiguous United States was in early 1979. Totality lasted for a maximum of 2 minutes 49 seconds, and the total eclipse was visible on a narrow path stretching from the Pacific Northwest to Greenland. Agencies from Canada and the United States – including NASA – joined forces to build a sounding rocket program to study the atmosphere and ionosphere during the eclipse by observing particles on the edge of space as the Sun’s radiation was suddenly blocked.

July 31, 1981

The USSR got a great view of the Moon passing in front of the Sun in the summer of 1981, with totality lasting just over 2 minutes at maximum. Our scientists partnered with Hawaiian and British researchers to study the Sun’s atmosphere – specifically, a relatively thin region called the chromosphere, which is sandwiched between the Sun’s visible surface and the corona – using an infrared telescope aboard the Kuiper Airborne Observatory. The chromosphere appears as the red rim of the solar disk during a total solar eclipse, whereas the corona has no discernible color to the naked eye.

Watch an Eclipse: August 21, 2017 

On August 21, a total solar eclipse will cross the continental United States from coast to coast for the first time in 99 years, and you can watch.

If skies are clear, people in North America will be able to see a partial or total solar eclipse. Find out what the eclipse will look like in your area, then make sure you have a safe method to watch – like solar viewing glasses or a pinhole projector – and head outside. 

You can also tune into nasa.gov/eclipselive throughout the day on Aug. 21 to see the eclipse like you’ve never seen it before – including a NASA TV show, views from our spacecraft, aircraft, and more than 50 high-altitude balloons.

Get all your eclipse information at https://eclipse2017.nasa.gov/, and follow along with @NASASun on Twitter and NASA Sun Science on Facebook.

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Today we successfully tested one of our RS-25 engines, four of which will help power our Space Launch System (SLS) to deep space destinations, like Mars! This 500-second engine test concludes a summer of successful hot fire testing for flight controllers at our Stennis Space Center near Bay St. Louis, Mississippi.

The controller serves as the “brain” of the engine, communicating with SLS flight computers to ensure engines are performing at needed levels. The test marked another step toward the nation’s return to human deep-space exploration missions.

We launched a series of summer tests with a second flight controller unit hot fire at the end of May, then followed up with three additional tests. The flight controller tests are critical preparation for upcoming SLS flights to deep space– the uncrewed Exploration Mission-1 (EM-1), which will serve as the first flight for the new rocket carrying an uncrewed Orion spacecraft, and EM-2, which will transport a crew of astronauts aboard the Orion spacecraft. 

Each SLS rocket is powered at launch by four RS-25 engines firing simultaneously and working in conjunction with a pair of solid rocket boosters. The engines generate a combined 2 million pounds of thrust at liftoff. With the boosters, total thrust at liftoff will exceed 8 million pounds!

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Black Hole Sculpts an Hourglass Galaxy

When it comes to galaxies, our home, the Milky Way, is rather neat and orderly. Other galaxies can be much more chaotic. For example, the Markarian 573 galaxy has a black hole at its center which is spewing beams of light in opposite directions, giving its inner regions more of an hourglass shape. 

Our scientists have long been fascinated by this unusual structure, seen above in optical light from the Hubble Space Telescope. Now their search has taken them deeper than ever — all the way into the super-sized black hole at the center of one galaxy.

So, what do we think is going on? When the black hole gobbles up matter, it releases a form of high-energy light called radiation (particularly in the form of X-rays), causing abnormal patterns in the flow of gas. 

Let’s take a closer look.

Meet Markarian 573, the galaxy at the center of this image from the Sloan Digital Sky Survey, located about 240 million light-years away from Earth in the constellation Cetus. It’s the galaxy’s odd structure and the unusual motions of its components that inspire our scientists to study it.

As is the case with other so-called active galaxies, the ginormous black hole at the center of Markarian 573 likes to eat stuff. A thick ring of dust and gas accumulates around it, forming a doughnut. This ring only permits light to escape the black hole in two cone-shaped regions within the flat plane of the galaxy — and that’s what creates the hourglass, as shown in the illustration above.

Zooming out, we can see the two cones of emission (shown in gold in the animation above) spill into the galaxy's spiral arms (blue). As the galaxy rotates, gas clouds in the arms sweep through this radiation, which makes them light up so our scientists can track their movements from Earth.

What happens next depends on how close the gas is to the black hole. Gas that’s about 2,500 light-years from the black hole picks up speed and streams outward (shown as darker red and blue arrows). Gas that’s farther from the black hole also becomes ionized, but is not driven away and continues its motion around the galaxy as before.

Here is an actual snapshot of the inner region of Markarian 573, combining X-ray data (blue) from our Chandra X-ray Observatory and radio observations (purple) from the Karl G. Jansky Very Large Array in New Mexico with a visible light image (gold) from our Hubble Space Telescope. Given its strange appearance, we’re left to wonder: what other funky shapes might far-off galaxies take?

For more information about the bizarre structure of Markarian 573, visit http://svs.gsfc.nasa.gov/12657  

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“I felt I was an accepted team member. It was a great experience and a unique opportunity.”

Ruth Ann Strunk, a math major, was hired in 1968 at NASA’s Kennedy Space Center as an acceptance checkout equipment software engineer. She monitored the work of contractors who wrote the computer programs designed to check out the command module, lunar module and the Apollo J mission experiments. These experiments were conducted aboard the service modules on Apollo 15, 16 and 17 by the command module pilots. 

“I am proud of the advancement and the number of women who are working and enjoy working here,” Strunk said. “It was a wonderful opportunity NASA afforded me during Apollo that I have been able to use ever since.”

Remember the women who made #Apollo50th possible.

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5 Reasons our Space Launch System is the Backbone for Deep Space Exploration

Our Space Launch System (SLS) will be the world’s most powerful rocket, engineered to carry astronauts and cargo farther and faster than any rocket ever built. Here are five reasons it is the backbone of bold, deep space exploration missions.

5. We’re Building This Rocket to Take Humans to the Moon and Beyond

The SLS rocket is a national asset for leading new missions to deep space. More than 1,000 large and small companies in 44 states are building the rocket that will take humans to the Moon. Work on SLS has an economic impact of $5.7 billion and generates 32,000 jobs. Small businesses across the U.S. supply 40 percent of the raw materials for the rocket. An investment in SLS is an investment in human spaceflight and in American industry and will lead to applications beyond NASA.

4. This Rocket is Built for Humans

Modern deep space systems are designed and built to keep humans safe from launch to landing.  SLS provides the power to safely send the Orion spacecraft and astronauts to the Moon. Orion, powered by the European Service Module, keeps the crew safe during the mission. Exploration Ground Systems at NASA’s Kennedy Space Center in Florida, safely launches the SLS with Orion on top and recovers the astronauts and Orion after splashdown.

3. This Rocket is Engineered for a Variety of Exploration Missions

SLS is engineered for decades of human space exploration to come. SLS is not just one rocket but a transportation system that evolves to meet the needs of a variety of missions. The rocket can send more than 26 metric tons (57,000 pounds) to the Moon and can evolve to send up to 45 metric tons (99,000 pounds) to the Moon. NASA has the expertise to meet the challenges of designing and building a new, complex rocket that evolves over time while developing our nation’s capability to extend human existence into deep space.

2. This Rocket can Carry Crews and Cargos Farther, Faster

SLS’s versatile design enables it to carry astronauts their supplies as well as cargo for resupply and send science missions far in the solar system. With its power and unprecedented ability to transport heavy and large volume science payloads in a single mission, SLS can send cargos to Mars or probes even farther out in the solar system, such as to Jupiter’s moon Europa, faster than any other rocket flying today. The rocket’s large cargo volume makes it possible to design planetary probes, telescopes and other scientific instruments with fewer complex mechanical parts.

1. This Rocket Complements International and Commercial Partners

The Space Launch System is the right rocket to enable exploration on and around the Moon and even longer missions away from home. SLS makes it possible for astronauts to bring along supplies and equipment needed to explore, such as pieces of the Gateway, which will be the cornerstone of sustainable lunar exploration. SLS’s ability to launch both people and payloads to deep space in a single mission makes space travel safer and more efficient. With no buildings, hardware or grocery stores on the Moon or Mars, there are plenty of opportunities for support by other rockets. SLS and contributions by international and commercial partners will make it possible to return to the Moon and create a springboard for exploration of other areas in the solar system where we can discover and expand knowledge for the benefit of humanity.

Learn more about the Space Launch System.

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Hello! Jeanette Epps here ready to take your @nasa questions!

How Well Do You Know Venus?

Similar in structure and size to Earth, Venus’ thick, toxic atmosphere traps heat in a runaway greenhouse effect. A permanent layer of clouds traps heat, creating surface temperatures hot enough to melt lead.

How did Venus get its name? It is named for the ancient Roman goddess of love and beauty. It is believed that Venus was named for the most beautiful of the ancient gods because it shone the brightest of the five planets known to ancient astronomers.

Here are a few fun facts that you might not know:

One day on Venus lasts as long as 243 Earth days (aka the time it takes for Venus to rotate or spin once)

Venus is a rocky planet, also known as a terrestrial planet

Venus’ thick and toxic atmosphere is made up mostly of carbon dioxide and nitrogen, with clouds of sulfuric acid droplets

Venus has no moons or rings

More than 40 spacecraft have explored the planet

No evidence of life has been found on Venus. The planet’s extreme high temperatures of almost 480 degrees Celsius (900 degrees Fahrenheit) makes it seem an unlikely place for life as we know it

Venus spins backwards when compared to the other planets. This means that the sun rises in the west and sets in the east

Night Light

Did you know that Venus is the brightest planet in Earth’s dark skies? Only the moon — which is not a planet — is brighter. Venus outshines the other planets because it is closer and its thick cloud cover is excellent at reflecting sunlight.

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The United Launch Alliance’s Atlas V rocket carrying the Orbital ATK Cygnus module rolls to Cape Canaveral Air Force Station's Launch Pad 41 in this time-lapse video. The rollout is in preparation for the Orbital ATK CRS-7 mission to deliver supplies to the International Space Station.

Launch is currently scheduled for 11:11 a.m. EDT, watch live coverage: http://www.nasa.gov/live 

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Observing the Ozone Hole from Space: A Science Success Story

Using our unique ability to view Earth from space, we are working together with NOAA to monitor an emerging success story – the shrinking ozone hole over Antarctica.

Thirty years ago, the nations of the world agreed to the landmark ‘Montreal Protocol on Substances that Deplete the Ozone Layer.’ The Protocol limited the release of ozone-depleting chlorofluorocarbons (CFCs) into the atmosphere.

Since the 1960s our scientists have worked with NOAA researchers to study the ozone layer. 

We use a combination of satellite, aircraft and balloon measurements of the atmosphere.

The ozone layer acts like a sunscreen for Earth, blocking harmful ultraviolet, or UV, rays emitted by the Sun.

In 1985, scientists first reported a hole forming in the ozone layer over Antarctica. It formed over Antarctica because the Earth’s atmospheric circulation traps air over Antarctica.  This air contains chlorine released from the CFCs and thus it rapidly depletes the ozone.

Because colder temperatures speed up the process of CFCs breaking up and releasing chlorine more quickly, the ozone hole fluctuates with temperature. The hole shrinks during the warmer summer months and grows larger during the southern winter. In September 2006, the ozone hole reached a record large extent.

But things have been improving in the 30 years since the Montreal Protocol. Thanks to the agreement, the concentration of CFCs in the atmosphere has been decreasing, and the ozone hole maximum has been smaller since 2006’s record.

That being said, the ozone hole still exists and fluctuates depending on temperature because CFCs have very long lifetimes. So, they still exist in our atmosphere and continue to deplete the ozone layer.

To get a view of what the ozone hole would have looked like if the world had not come to the agreement to limit CFCs, our scientists developed computer models. These show that by 2065, much of Earth would have had almost no ozone layer at all.

Luckily, the Montreal Protocol exists, and we’ve managed to save our protective ozone layer. Looking into the future, our scientists project that by 2065, the ozone hole will have returned to the same size it was thirty years ago.

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